Radiometric Temperature Determination in Nongray Bridgmanite: Applications to Melting Curve and Post‐Perovskite Transition Boundary in the Lower Mantle-Reference-Cited by-同舟云学术

Radiometric Temperature Determination in Nongray Bridgmanite: Applications to Melting Curve and Post‐Perovskite Transition Boundary in the Lower Mantle

Published:2021-05 Issue:5 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Lobanov Sergey S.¹²^ORCID,Speziale Sergio¹^ORCID,Lin Jung‐Fu³^ORCID,Schifferle Lukas¹²^ORCID,Schreiber Anja¹

Affiliation:

1. GFZ German Research Centre for Geosciences Telegrafenberg, Potsdam Germany

2. Insitute of Geosciences University of Potsdam Karl‐Liebknecht‐Straße, Potsdam Germany

3. Department of Geological Sciences Jackson School of Geosciences The University of Texas at Austin Austin TX USA

Funder

Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB021723

Reference70 articles.

1. Pressure calibration of diamond anvil Raman gauge to 310GPa

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3. Solidus and liquidus profiles of chondritic mantle: Implication for melting of the Earth across its history

4. Melting of subducted basalt at the core-mantle boundary

5. Achieving accuracy in spectroradiometric measurements of temperature in the laser-heated diamond anvil cell: Diamond is an optical component

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